Out of this world: giant supervolcanoes found on ancient Mars

Titanic eruptions may have played critical role in formation of planet’s early atmosphere millions of years ago

Steve Connor
Thursday 03 October 2013 12:41
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This image shows digital elevation data overlaid on daytime thermal infrared images of Eden Patera, the type example of an ancient supervolcano on Mars. Red colors are relatively high and purple-gray colors are low. The caldera is approximately 1800 metre
This image shows digital elevation data overlaid on daytime thermal infrared images of Eden Patera, the type example of an ancient supervolcano on Mars. Red colors are relatively high and purple-gray colors are low. The caldera is approximately 1800 metre

Giant “supervolcanoes” that could eject 1,000 cubic kilometres of material in one massive eruption – about 200 times the size of the Mount Pinatubo eruption in the Philippines in 1991 – has been discovered on Mars.

Scientists said that the supervolcanoes, which are now extinct, may have played a critical role in the formation of the planet’s early atmosphere many millions of years ago when the planet could have supported microbial life-forms.

Features typical of supervolcanoes, which erupt suddenly with immense energy and do not leave cone-shaped mountains behind like the more slowly erupting volcanoes on Earth, have been discovered in an area of Mars not previously thought to be volcanic, said Joseph Michalksi of the Natural History Museum in London and the Planetary Institute in Tucson, Arizona.

“The atmosphere of any planet including our own comes largely from volcanic outgassing. If we want to know about the early phase of that we need to know about these early volcanoes and this discovery gives us an early window into that process,” Dr Michalski said.

One of the examples of a Martian supervolcano is the Eden Patera, an irregularly-shaped crater in an area of Mars called the Arabia Terra. Discovering such supervolcanic structures “fundamentally changes how we view ancient volcanism on Mars”, said Dr Michalksi, who led the study published in the journal Nature.

“Many Martian volcanoes are easily recognised from their massive shield-shaped structure, similar to what we see in Hawaii. But, these are relatively youthful features on Mars and we have always wondered where the ancient volcanoes are. It is possible that the most ancient volcanoes were much more explosive and formed structures similar to what we now see in Arabia Terra,” Dr Michalksi said.

This image shows a 3-dimensional view of Eden Patera looking toward the east. Color image data from the High Resolution Stereo Camera (HRSC) were draped over digital topographic data from the same instrument

“It makes sense that supervolcanoes might have been more common on ancient Mars, particularly if the ancient crust was thinner than it is now. This would allow magma to rise to the surface more quickly, before it could release gases within the crust,” he said.

“If future work shows that supervolcanoes were present more widely on ancient Mars, it would completely change estimates of how the atmosphere formed from volcanic gases, how sediments formed from volcanic ash and how habitable the surface might have been.

This image shows a high-resolution view of layered materials and collapse features on the floor of Eden Patera. The layers represent areas where lava in an ancient lava lake attached to ridges and hills in the floor of the crater, froze against the bedrock, and then detached as the lava lake drained from beneath

“Volcanism is the thread binding nearly every aspect of Mars’ geologic evolution. The better we understand volcanism on Mars, the better we can understand the planet as a complex system,” he added.

Supervolcanoes also exist on Earth, such as at Yellowstone National Park in Wyoming and Toba in Indonesia, which erupted about 73,000 years ago and caused a period of extensive global cooling for many years.

This image shows another candidate supervolcano on Mars, called Oxus Patera. The image was created by draping color images from the High Resolution Stereo Camera draped over digital elevation data from the same instrument. Notice the irregular basins within the crater that represent multiple stages of collapse. Mountains within the 30-km-diametre crater are composed of fine-grained, friable materials that may represent volcanic ash deposits

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